Forts, Floods, and Periglacial Features: Exploring the Pittsburgh Low Plateau and Upper Youghiogheny Basin

This guidebook provides detailed itineraries of three of the geological field trips related to the 2017 joint meeting of the GSA Northeastern and North-Central Sections in Pittsburgh. The first chapter outlines a walking trip of downtown Pittsburgh and the escarpment to its south, consisting of seven “Pitt stops” investigating geological, archaeological, and historical aspects of the Gateway to the West. Venturing further afield, the second chapter describes a trip that explores periglacial features as far as the Upper Youghiogheny River basin in Maryland and the Laurel Highlands of Pennsylvania. The third chapter investigates hydrologic aspects of the 1889 Johnstown, Pennsylvania, flood, largely following the progress of the flood from its point of origin to the city of Johnstown.
Pleistocene periglacial features of the Pittsburgh Low Plateau and Upper Youghiogheny Basin
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Published:January 01, 2017
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CiteCitation
Rebecca Kavage Adams, Mark D. Swift, David K. Brezinski, Steven J. Kite, 2017. "Pleistocene periglacial features of the Pittsburgh Low Plateau and Upper Youghiogheny Basin", Forts, Floods, and Periglacial Features: Exploring the Pittsburgh Low Plateau and Upper Youghiogheny Basin, Joseph T. Hannibal, Kyle C. Fredrick
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Abstract
During the Pleistocene, the Laurentian Ice Sheet extended southward into western Pennsylvania. This field trip identifies a number of periglacial features from the Pittsburgh Low Plateau section to the Allegheny Mountain section of the Appalachian Plateaus Province that formed near the Pleistocene ice sheet front. Evidence of Pleistocene periglacial climate in this area includes glacial lake deposits in the Monongahela River valley near Morgantown, West Virginia, and Sphagnum peat bogs, rock cities, and patterned ground in plateau areas surrounding the Upper Youghiogheny River basin in Garrett County, Maryland, and the Laurel Highlands of Somerset County, Pennsylvania. In the high lying basins of the Allegheny Mountains, Pleistocene peat bogs still harbor species characteristic of more northerly latitudes due to local frost pocket conditions.
- Allegheny Mountains
- Allegheny Plateau
- Appalachians
- bogs
- Cenozoic
- drainage basins
- field trips
- fractures
- geomorphology
- glacial geology
- joints
- last glacial maximum
- mires
- Monongalia County West Virginia
- North America
- patterned ground
- Pennsylvania
- periglacial features
- Pleistocene
- Preston County West Virginia
- Quaternary
- road log
- sedimentation
- Somerset County Pennsylvania
- United States
- West Virginia
- wetlands
- Monongahela Valley
- Upper Youghiogheny Basin
- Mount Davis
- Negro Mountain
- Dorsey Knob Park
- Snaggy Mountain
- Pittsburg Low Plateau
- Markleton Quadrangle